Continental Collision
Continental Collision is a tectonic plate interaction process in which two plates bearing buoyant continental lithosphere converge after the closure of an intervening ocean basin, terminating oceanic subduction and producing large-scale crustal thickening, deformation, and orogenesis.
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413
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Robert Reilinger, S. McClusky, Philippe Vernant et al. · Journal of Geophysical Research Atmospheres · 2006 · 2.1K citations · Full text
T. Mark Harrison, Peter Copeland, W. S. F. Kidd et al. · Science · 1992 · 1.3K citations
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Centre National de la Recherche Scientifique
Paris, France
57 h-index
313 publications
23.5K citations

Chinese Academy of Sciences
Beijing, China
57 h-index
349 publications
34.3K citations

Chinese Academy of Geological Sciences
Beijing, China
46 h-index
204 publications
25.8K citations
Institute of Geology and Geophysics
Beijing, China
45 h-index
199 publications
25.5K citations
ETH Zurich
Zurich, Switzerland
40 h-index
79 publications
9.2K citations

China University of Geosciences (Beijing)
Beijing, China
39 h-index
229 publications
24.4K citations

Sorbonne Université
Paris, France
33 h-index
80 publications
12.1K citations
China University of Geosciences
Wuhan, China
32 h-index
165 publications
9.2K citations
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JGR · 64 publications · 11.9K citations
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